Why Is The Sea Floor Spreading

The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate.

Why is the sea floor spreading.

This theory introduced by harry hess. These age data also allow the rate of seafloor spreading to be determined and they show that rates. This seafloor spreading hypothesis had been proposed a few years earlier by harry hess a petrologist at princeton university and robert dietz an oceanographer in the us coast and geodetic survey the federal department that made maps of the oceans and us coastlines. Due to this continuous seafloor spreading occurs and makes atlantic ocean floor to be connected to other continental crust making the ocean gets wider over the time.

Seafloor spreading is the mechanism by which new seafloor lithosphere is constantly being created at mid ocean ridges. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Spreading rates determine if the ridge is fast intermediate or slow. If the earth s crust was expanding along the oceanic ridges hess reasoned it must be shrinking elsewhere.

The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. Using new data analysis techniques nasa scientists have confirmed the earth isn t expanding putting to rest years of rumors that the earth is growing. Seafloor spreading is a geologic process where there is a gradual addition o.

This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century. Subduction and sea floor spreading are processes that could alter the size and form of the ocean. Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them. Dietz and hess were among the small handful who really understood the broad implications of sea floor spreading.

Hess went on to say that as the ocean crust spreads and cools over millions. For instance the atlantic ocean is believed to be expanding because of its few trenches.